V. Thermochemistry

Key focus of this chapter: enthalpy change

This chapter reviews enthalpy changes, internal energy, pressure–volume work, heat transfer, Hess’s law, entropy, and Gibbs free energy.

Thermochemistry: the study of heat absorbed or released during chemical reactions and physical changes.

A. Energy (E)

: ability to do work (W) or transfer heat (Q).

ΔE (change in internal energy) = Efinal -Einitial

  • System: the part of the universe selected for study, such as the reacting substances.
  • Surroundings: the rest of the universe
System and surroundings of enthalpy change

(+) energy

(-) energy

W

• Work is done on system

• Work is done by system

Q (heat)

Qp = ΔH at constant pressure, with only pressure–volume work.

• Absorbing heat into system

  from surroundings

• Releasing heat from system to

  surroundings

  • Question: What is ΔE when a system does 100 J of work and releases 80 J of heat?

ΔE = W + Q

= (-100J) + (-80J)

= -180J

B. Pressure–volume work

1. Pressure

Pressure equals force divided by area; pressure is measured in pascals, Pa.
  • 1 atm = 760 mmHg (torr)

2. Work (W)

: pressure–volume work is W = −PextΔV at constant external pressure. More generally, mechanical work is force times displacement in the direction of the force.

+W

• Work is done on system

• - ΔV (contraction of volume)

• External pressure compresses

the system

- W

• Work is done by system

• + ΔV (expansion of volume)

• The system expands against

external pressure

  • Question: What is the work when a gas expands from 8.0 L to 10.0 L against an external pressure of 3.0 atm?

W = −PextΔV (work is done by system)

= – 3 atm × (10.0 – 8.0 ) L

= −6.0 L·atm ≈ −6.1 × 102 J

C. Heat energy, Q

  • Calorie: approximately the energy required to raise the temperature of 1 g of water by 1 °C

** 1 cal = 4.184 J

  • Specific heat capacity, C: the heat required to raise the temperature of one gram of a substance by one degree Celsius (or one kelvin).

     ** Specific heat of water is 4.18 J/(g·°C)

  •  Question: Calculate the heat energy to raise the temperature of 100 g of water from 50 °C to 80 °C.

Q = C·m·ΔT

= 4.18 J/(g·°C) × 100 g × (80-50) °C

= 12,540 J

  • Question: Calculate the specific heat of gold when 650 J of heat is used to increase the temperature of 50 g of gold from 25 °C to 125 °C.

D. Laws of thermodynamics

First law


• Law of conservation of energy: the total energy of a system and its surroundings is neither created nor destroyed.

Second law


• In a spontaneous process, the total entropy of the system and surroundings increases: ΔSuniv > 0. For a reversible process, ΔSuniv = 0.

E. Enthalpy change, ΔH

: ΔH = Hfinal – Hinitial

Exothermic processes, ΔH < 0


Endothermic processes, ΔH > 0


Diagrams

Graph and equation

System

• Giving off heat to surroundings

• The system loses energy as heat; enthalpy decreases at constant pressure

• Bond formation processes

• State change: gas → liquid → solid

• Getting heat from surroundings

• The system gains energy as heat; enthalpy increases at constant pressure

• Bond breaking processes

• State change: solid → liquid → gas

Surroundings

• Surroundings receive heat

• Surroundings supply heat

Examples

• Combustion of fuel, acid and base neutralization, catabolism of glucose in a cell, mixing water with strong acids

• Melting solid salts, producing glucose by photosynthesis, cold pack by mixing water with ammonium nitrate

** The total energy of the system and its surroundings is conserved in both exothermic and endothermic processes.

F. Hess’s Law

  • The ΔH of an overall reaction is equal to the sum of the ΔH of the individual steps.
  • Enthalpy is a state function: its change depends only on the initial and final states, not on the pathway. Reversing a reaction changes the sign of ΔH; multiplying an equation by a factor multiplies ΔH by the same factor.
Conservation of energy. Hess law: -2 + -3 = -5; equation (1) + (2) = (3).
  • Question: Calculate the energy change, ΔH, for the reaction S(s) + O2(g) → SO2(g) from the following information.

For this calculation exercise, use the supplied hypothetical reaction enthalpies for the equations as written. These values are not tabulated standard formation enthalpies.

Table A

Solution:

Table A

1/2 × 1st reaction

Reverse direction of 2nd reaction

1st reaction +

 2nd reaction

Therefore, the energy change of the reaction S(s) + O2(g) → SO2(g) is +5 kJ/mol.

G. Measuring enthalpy change, ΔHo

: calculate reaction enthalpy from standard enthalpies of formation or estimate it from average bond energies. The standard enthalpy of formation, ΔH°f, refers to forming one mole of a substance from its elements in their reference states.

Question: Using the supplied rounded formation enthalpies, calculate ΔHo for the reaction.

CH4(g) + 2O2(g)   →  CO2(g) + 2H2O(l)

Molecules

-75

-390

-290

Solution: Using the supplied rounded values, ΔHo = Σ products of ΔHof  – Σ reactants of ΔHof

     = [CO2 + 2H2O] – [CH4]         ** ΔHof of O2 = 0 kJ/mol

     =[(-390) + 2(-290)] – (-75)

= −895 kJ for the reaction as written. Multiply each standard formation enthalpy by its stoichiometric coefficient; O2(g), an element in its reference state, has ΔH°f = 0.

Question: Estimate ΔH for the gas-phase reaction using the average bond dissociation energies in Table B.

2C2H6(g) + 7O2(g)  →  4CO2(g)  + 6H2O(g)

Table B

Bonds

Average bond dissociation energies (kJ/mol)


C-H

410

C-C

350

O=O

500

C=O

730

O-H

460

Solution: Σ (Bond energies of reactants) – Σ (Bond energies of products)

= [(C-H)×12 + (C-C)×2 + (O=O)×7] – [(C=O)×8+(O-H)×12]

= [410×12 + 350×2 + 500×7] –[730×8+460×12]

= -2,240kJ

H. Entropy change, ΔS

ΔS > 0

ΔS < 0

Examples of system entropy increase; many but not all dissolution processes increase entropy.
  • ΔS = ∑ (entropy of products) – ∑ (entropy of reactants)

Question: Calculate ΔS for this hypothetical reaction using the supplied molar entropies in J/(mol·K).

W + X  →  Y + Z

S

W

3

X

2

Y

5

Z

4

ΔS = (Y + Z) – (W+X)

= (5+4) – (3 +2)

= 4 J/(mol·K)

  • Entropy of the surroundings, ΔSsurr

Increasing entropy of surroundings

Decreasing entropy of surroundings

I. Gibbs free energy change, ΔG

: at constant temperature and pressure, ΔG determines whether a process is thermodynamically favorable in the forward direction. ΔG < 0 is favorable, ΔG = 0 indicates equilibrium, and ΔG > 0 favors the reverse direction. Thermodynamic favorability does not determine reaction speed.

  • ΔH < 0 and ΔS >0 at T > 0 is always a spontaneous reaction.

Question: For these hypothetical values, which choices represent a thermodynamically favorable reaction at T = 1 K? Use ΔH in kJ/mol and ΔS in kJ/(mol·K).

A. ΔH = -1, ΔS = -2

B. ΔH = +1, ΔS = -2

C. ΔH = +1, ΔS = +2

D. ΔH = -1, ΔS = +2

E. C and D

ANS: E

Solution: For ΔG = ΔH – TΔS

A. -1 – (-2) = +1

B. +1 – (-2) = +3

C. +1 – (+2) = -1

D. -1 – (+2) = -3

Question: For a hypothetical process with ΔH = 6 J/mol and ΔS = 3 J/(mol·K), calculate the equilibrium temperature in kelvin.